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danielandpenn
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I'm curious as to why there aren't heavier metals in the Earth's core than iron and nickel. Why those two? Anyone have any insight?
danielandpenn said:I'm curious as to why there aren't heavier metals in the Earth's core than iron and nickel. Why those two? Anyone have any insight?
The core of the Earth is still hot because it contains radioactive uranium and thorium atoms. Although the core is mostly iron, it also contains most of the Earth's uranium.
Andre said:Welcome, Danie
What happens in the core is all pure hypothetical, since we have only some very indirect observations. The wiki ref of tiny-tim is certainly true qualitatively but there is no way of quantifying the concentration of heavy elements in the core as well as their contribution to the terrestrial generated heat. There are more hypotheses going around, none of which can be selected as being the right one.
The iron - nickle abundance is no doubt related to the total abundance of those elements in the solar system, whereas the heavy elements are much more rare.
Another element could be, the order in which compounds became fluid or not, during the -hypothetical- http://www.hopkins.k12.mn.us/pages/high/courses/online/astro/course_documents/earth_moon/earth/geologic_time/iron_catastrophe.htm
But in the end it's all a sophisticated guess.
Gold isn't very chemically active but is soluable at very high pressures. It is carried along cracks by steam/fluids from volcanoes and is deposited out as they cool. So are lots of other metals, there a bunch of elements like platinum and telurium that you find along with gold.baywax said:... and that is why is gold associated with volcanic activity?
mgb_phys said:Gold isn't very chemically active but is soluable at very high pressures. It is carried along cracks by steam/fluids from volcanoes and is deposited out as they cool. So are lots of other metals, there a bunch of elements like platinum and telurium that you find along with gold.
Almanzo said:If the core of Jupiter is made of diamond, that would mean that carbon is dominating Jupiter's core. One would have to conclude that elements heavier than carbon (such as iron and nickel) are relatively rare on Jupiter. In that case iron and nickel cannot be all that common in the Solar System, and one would have to wonder why they are common on Earth.
That is quite different from the case for hydrogen. Hydrogen is the most common element in the universe, but Earth cannot keep hold of it (except in compounds with heavier elements, such as oxygen), because it is light enough to escape from Earth's gravity well. Jupiter is more massive, and was therefore able to retain more hydrogen.
Carbon, however, would not escape from Earth, at least not over the present age of the Solar System. If a large part of Jupiter is made of carbon, that would be strange.
We don't have direct seismic data for Mars but it is thought to be similair to Earth. The difference is that Mars is smaller and so it's core cooled and solidifed and so has no (significant) magnetic field.baywax said:Do we know what the predominant metal/other is at Mar's core?
The volcanic activity of Io is due to the energy input from Jupiter, from tidal forces, it is too small to have a liquid core purely from internal heat sources. It does look like it has an iron core from magnetic field measurements made by the Galileo probe.Does the volcanic activity of Io, next to Jupiter, indicate a core content similar to earth's?
baywax said:Gee, I thought it was one big diamond at the centre... or is that Jupiter
To my knowledge, there is no real evidence of any significant amounts of carbon in Jupiter's core. The diamond core theory was made up by Arthur C. Clarke for one of his later Odyssey novels.Almanzo said:If the core of Jupiter is made of diamond, that would mean that carbon is dominating Jupiter's core.
Gokul43201 said:To my knowledge, there is no real evidence of any significant amounts of carbon in Jupiter's core. The diamond core theory was made up by Arthur C. Clarke for one of his later Odyssey novels.
There is definitely more realistic speculation of metallic hydrogen in jupiter's core, but I don't think that's been verified either.
You need oxygen for things to burn, also Carbon has a rather high boiling point (4000K)sketchtrack said:Wouldn't it be too hot for diamonds in the core of a planet?
mgb_phys said:You need oxygen for things to burn and Carbon has a rather high boiling point (4000K)
Diamond isn't the most stable form of Carbon, diamonds (slowly) decay into graphite at room temperature - I don't know about at the pressure in the centre of a planet
sketchtrack said:Could one assume that if there is carbon in or near the core, it is probably in diamond form?
Elementally the iron and nickel would not be different, but given a pressure of about 350 GPa, the distances between nuclei, or lattice parameters of any crystal arrangement would be very small. But the core is considered to be liquid.danielandpenn said:Are you saying that the nickel and iron in the core may be different from the nickel and iron as we know it because of the intense pressure and temps?
gdp said:There is another point that has not yet been raised except in passing, which is that in nature, because the various elements have various chemical affinities for each other, most elements in nature do not occur in "pure" form, but rather in the form of chemical compounds or mixtures.
The Earth's core is believed to be mostly composed of a mixture of http://en.wikipedia.org/wiki/Goldschmidt_classification#Siderophile_elements" In addition to iron, cobalt, and nickel, the siderophiles include manganese, molybdenum, gold, and the platinum and palladium group elements.
Secondarily, in the core one also expects to find enhanced abundances of the http://en.wikipedia.org/wiki/Goldschmidt_classification#Chalcophile_elements" --- most notably sulfur itself, which is believed by some to be a significant constituent of the liquid "outer core." (Mercury, BTW, happens to be a chalcophile.)
By contrast, uranium and most uranium compounds are http://en.wikipedia.org/wiki/Goldschmidt_classification#Lithophile_elements" and are therefore believed to have become largely concentrated mostly in the Earth's lithosphere (i.,e., its "crust"), rather than in its mantle or core --- despite the relatively high specific gravities of uranium and most of its compounds. [Note that chemical bonds are basically `electromagnetic' in nature, and that gravity is actually an extremely weak force compared to the electromagnetic force. (Relatively speaking, the electromagnetic force is about ~1040 times stronger than the gravitational force.) Hence, the chemical bonds between uranium and the other lithophilic elements are easily capable of preventing uranium from sinking to the core under the influence of the Earth's relatively weak gravitational field.]
There is a heterodox hypothesis by maverick nuclear chemist http://en.wikipedia.org/wiki/J._Marvin_Herndon" that the core is primarily composed of nickel silicide rather than metallic nickel-iron alloy. Nickel silicide has enough of an affinity for uranium that, despite uranium's relatively low cosmic abundance, there might have been enough uranium dissolved in the primitive core for it to later separate out to form a small innermost "kernel" of uranium or uranium sulfide with a diameter of ~1--10 km at the center of the inner core. Herndon also believes that this inner "kernel" functions as an intermittent fast fission reactor that drives various geological processes. However, very few "mainstream" geologists take Herndon's "nuclear planet" hypothesis seriously, and there is currently very little evidence of even a circumstantial nature to support it.
danielandpenn said:Wow! How do you know all this GDP? I can really grasp that! Thanks.
DrClapeyron said:By which process is uranium created? Which process is iron created?
Simply, iron production was favored during the formation of our early solar nebula. Chalk it up to thermodynamics.
Better question: why is the Earth's core iron and its mantle silicate?
Sounds much like the separation of the slag on top of liquid iron in the iron and steel making process.gdp said:Quite simply, because they are mutually immiscible substances, and the iron fraction is denser than the silicate fraction. The two fractions separated in the primordial molten Earth for exactly the same reason that oil and vinegar separate in a bottle of salad dressing.
Astronuc said:Sounds much like the separation of the slag on top of liquid iron in the iron and steel making process.
http://www.tfhrc.gov/hnr20/recycle/waste/ssa1.htm
The Earth's core is primarily composed of iron and nickel. These elements make up about 85% of the core's mass and are responsible for its magnetic field.
Scientists use a variety of methods to study the Earth's core, including seismic waves, magnetic field measurements, and laboratory experiments. These techniques provide insight into the composition and physical properties of the core.
The study of iron and nickel in the Earth's core is important because these elements play a crucial role in the planet's formation and evolution. Understanding their properties and behavior can help us better understand the processes that shaped the Earth and continue to shape it today.
Iron and nickel are thought to have been present in the early Earth as it formed from the solar nebula. As the planet grew and differentiated, these heavier elements sank towards the center due to their higher density, eventually forming the core.
There are several theories about the Earth's core, including the dynamo theory which explains the origin of the magnetic field, the inner core nucleation theory which suggests that the inner core formed much later than the rest of the core, and the core-mantle interaction theory which proposes that the core and mantle are continuously exchanging materials and energy.